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Effects of shoal margin collapses on the morphodynamics of a sandy estuary
van Dijk, W.M.; Hiatt, M.R.; van der Werf, J.J.; Kleinhans, M.G. (2019). Effects of shoal margin collapses on the morphodynamics of a sandy estuary. JGR: Earth Surface 124(1): 195-215.
In: Journal of Geophysical Research-Earth Surface. AMER GEOPHYSICAL UNION: Washington. ISSN 2169-9003; e-ISSN 2169-9011, meer
Peer reviewed article  

Beschikbaar in  Auteurs 

    Marien; Brak water; Zoet water
Author keywords
    estuary; shoal margin collapse; channel-shoal morphodynamics; tidalbars; Western Scheldt; channel network

Auteurs  Top 
  • van Dijk, W.M.
  • Hiatt, M.R.
  • van der Werf, J.J., meer
  • Kleinhans, M.G., meer

    Shoal margin collapses of several million cubic meters have occurred in the Western Scheldt estuary, the Netherlands, on average five times a year over the last decades. While these collapses involve significant volumes of material, their effect on the channel-shoal morphology is unknown. We hypothesize that collapses dynamicize the channel-shoal interactions, which could impact the ecological functioning, flood safety, and navigation in the estuary. The objective is to investigate how locations, probability, type, and volume of shoal margin collapse affect the channel-shoal dynamics. We implemented an empirically validated parameterization for shoal margin collapses and tested its effect on simulated estuary morphological development in a Delft3D schematization of the Western Scheldt. Three sets of scenarios were analyzed for near-field and far-field effects on flow pattern and channel-shoal morphology: (1) an observed shoal margin collapse of 2014, (2) initial large collapses on 10 locations, and (3) continuous collapses predicted by our novel probabilistic model over a time span of decades. Results show that a single shoal margin collapse only affects the local dynamics in the longitudinal flow direction and dampen out within a year for typical volumes, whereas larger disturbances that reach the seaward or landward sill at tidal channel junctions grow. The direction of the strongest tidally averaged flow determined the redistribution of the collapsed sediment. We conclude that adding the process of shoal margin collapses increases the channel-shoal interactions and that in intensively dredged estuaries shoal margins oversteepen, amplifying the number of collapses, but because of dredging the natural morphological response is interrupted.

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